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The '''Grwyne Fawr''' is a river in the | [[File:The Grwyne Fawr below the reservoir dam spillway (geograph 3590134).jpg|right|thumb|230px|The Grwyne Fawr above the reservoir]] | ||
{{county|Brecknockshire}} | |||
The '''Grwyne Fawr''' is a river in the [[Black Mountains]], within the [[Brecon Beacons]] National Park. A section of it forms the border between two counties: [[Brecknockshire]] on the west bank and [[Monmouthshire]] on the east. | |||
The | The river and its major tributary the '''Grwyne Fechan''' flow into the [[River Usk]] at [[Glangrwyney]]. | ||
The name of the river probably originates from ''gweryn'' or ''gwerynau'' and ''mawr/fawr'' meaning 'large river at the wet place'.<ref>Owen, H.W. & Morgan, R. 2007 'Dictionary of the Place-names of Wales' Gomer Press</ref> | |||
The two rivers join near the village of Llanbedr and head south as the Grwyne Fawr through the hamlet of Llangenny to their confluence with the [[River Usk]] at Glangrwyney. | The Gwryne Fawr rises at Blaen Grwyne Fawr on the southern slopes of [[Rhos Dirion]] in the [[Black Mountains]] and follows a south-eastward course for several miles, its flow interrupted by the presence of the Grwyne Fawr Reservoir, the only waterbody within this range of hills. Some way below the reservoir, Mynydd Du Forest clothes the sides of the valley. Though a public road penetrates the valley as far as the north end of the forest, the valley is very sparsely populated. It is only approaching the hamlet of [[Partrishow]] that the valley takes on a farmed appearance. | ||
Below Partrishow the river heads west along a valley whose alignment is guided by the presence of a geological line of weakness known as the [[Neath Disturbance]]. | |||
[[File:Rhos dirion.JPG|left|thumb|300px|Rhos Dirion in the Black Mountains]] | |||
To the west, the Grwyne Fechan takes a parallel course to that of it larger neighbour. It rises on the southern slopes of [[Waun Fach]] and gathers a number of tributary streams from the broad ridge which separates it from the Grwyne Fawr. Though there are numerous conifer plantations, the valley has a more open aspect than that of the Grwyne Fawr. | |||
The two rivers join near the village of [[Llanbedr, Crickhowell|Llanbedr]] and head south as the Grwyne Fawr through the hamlet of [[Llangenny]] to their confluence with the [[River Usk]] at Glangrwyney. | |||
==Geology== | ==Geology== | ||
Both the Grwyne Fawr and the Grwyne Fechan drain the Old Red Sandstone hills of the Black Mountains. These are the Brownstones and Senni Formations which date from the Breconian stage of the Devonian period. The sandstones and mudstones of these formations can frequently be seen in the beds of the two rivers and sometimes exposed in the often steep valley sides. The lower reaches of the river run through an area blanketed with glacial till, a legacy of the last ice age.<ref>British Geological Survey 1:50,000 map sheets 214 'Talgarth' & 232 'Abergavenny' and accompanying memoir/sheet explanation</ref> | Both the Grwyne Fawr and the Grwyne Fechan drain the Old Red Sandstone hills of the Black Mountains. These are the Brownstones and Senni Formations which date from the Breconian stage of the Devonian period. The sandstones and mudstones of these formations can frequently be seen in the beds of the two rivers and sometimes exposed in the often steep valley sides. The lower reaches of the river run through an area blanketed with glacial till, a legacy of the last ice age.<ref>British Geological Survey 1:50,000 map sheets 214 'Talgarth' & 232 'Abergavenny' and accompanying memoir/sheet explanation</ref> | ||
==Historical interest== | |||
[[File:Llangenny bridge - geograph.org.uk - 1287624.jpg|right|thumb|230px|Llangenny Bridge on the Grwyne Fawr]] | |||
The valley of the Grwyne Fawr, then known as "Coed Grano", was the site of the murder in 1136 of the Norman Marcher lord Richard de Clare, 1st Earl of Hereford, by the Welsh under Iorwerth ab Owain and his brother Morgan, grandsons of Caradog ap Gruffydd. This resulted in a period of conflict between the Welsh princes and the Anglo-Norman lords in south Wales.<ref>[http://www.breconbeaconsparksociety.org/The%20Beacon/pstbBlackMountainMagic.htm Brecon Beacons Park Society]</ref> | |||
==Location== | |||
*Location map: {{wmap|51.833333|-3.1|zoom=14}} | |||
{{commons}} | |||
==References== | ==References== | ||
{{Reflist}} | {{Reflist}} | ||
[[Category:Rivers of Brecknockshire]] | [[Category:Rivers of Brecknockshire]] | ||
[[Category:Rivers of Monmouthshire]] | [[Category:Rivers of Monmouthshire]] | ||
Latest revision as of 22:45, 22 February 2018
.jpg)
The Grwyne Fawr is a river in the Black Mountains, within the Brecon Beacons National Park. A section of it forms the border between two counties: Brecknockshire on the west bank and Monmouthshire on the east.
The river and its major tributary the Grwyne Fechan flow into the River Usk at Glangrwyney.
The name of the river probably originates from gweryn or gwerynau and mawr/fawr meaning 'large river at the wet place'.[1]
The Gwryne Fawr rises at Blaen Grwyne Fawr on the southern slopes of Rhos Dirion in the Black Mountains and follows a south-eastward course for several miles, its flow interrupted by the presence of the Grwyne Fawr Reservoir, the only waterbody within this range of hills. Some way below the reservoir, Mynydd Du Forest clothes the sides of the valley. Though a public road penetrates the valley as far as the north end of the forest, the valley is very sparsely populated. It is only approaching the hamlet of Partrishow that the valley takes on a farmed appearance.
Below Partrishow the river heads west along a valley whose alignment is guided by the presence of a geological line of weakness known as the Neath Disturbance.
To the west, the Grwyne Fechan takes a parallel course to that of it larger neighbour. It rises on the southern slopes of Waun Fach and gathers a number of tributary streams from the broad ridge which separates it from the Grwyne Fawr. Though there are numerous conifer plantations, the valley has a more open aspect than that of the Grwyne Fawr.
The two rivers join near the village of Llanbedr and head south as the Grwyne Fawr through the hamlet of Llangenny to their confluence with the River Usk at Glangrwyney.
Geology
Both the Grwyne Fawr and the Grwyne Fechan drain the Old Red Sandstone hills of the Black Mountains. These are the Brownstones and Senni Formations which date from the Breconian stage of the Devonian period. The sandstones and mudstones of these formations can frequently be seen in the beds of the two rivers and sometimes exposed in the often steep valley sides. The lower reaches of the river run through an area blanketed with glacial till, a legacy of the last ice age.[2]
Historical interest
The valley of the Grwyne Fawr, then known as "Coed Grano", was the site of the murder in 1136 of the Norman Marcher lord Richard de Clare, 1st Earl of Hereford, by the Welsh under Iorwerth ab Owain and his brother Morgan, grandsons of Caradog ap Gruffydd. This resulted in a period of conflict between the Welsh princes and the Anglo-Norman lords in south Wales.[3]
Location
- Location map: 51°49’60"N, 3°6’0"W
 |
("Wikimedia Commons" has material about Grwyne Fawr) |
References
- ↑ Owen, H.W. & Morgan, R. 2007 'Dictionary of the Place-names of Wales' Gomer Press
- ↑ British Geological Survey 1:50,000 map sheets 214 'Talgarth' & 232 'Abergavenny' and accompanying memoir/sheet explanation
- ↑ Brecon Beacons Park Society